2013
DOI: 10.1109/tap.2013.2268244
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An Analytical Model of ELF Radiowave Propagation in Ground-Ionosphere Waveguides With a Multilayered Ground

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Cited by 13 publications
(14 citation statements)
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“…CM variation in the source process is reconstructed by correcting the measured signals for transformations caused by the recording system and the propagation in the Earth‐ionosphere spherical waveguide. Details of the method are discussed by Kulak et al (), Mlynarczyk et al (), and Mlynarczyk et al (). RSs are characterized by their CMC obtained from the maximum recorded amplitude of the corresponding extremely low frequency signals using the impulse approximation (iCMC; Berger et al, ; Kułak et al, ).…”
Section: Instrumentation Data and Methodsmentioning
confidence: 99%
“…CM variation in the source process is reconstructed by correcting the measured signals for transformations caused by the recording system and the propagation in the Earth‐ionosphere spherical waveguide. Details of the method are discussed by Kulak et al (), Mlynarczyk et al (), and Mlynarczyk et al (). RSs are characterized by their CMC obtained from the maximum recorded amplitude of the corresponding extremely low frequency signals using the impulse approximation (iCMC; Berger et al, ; Kułak et al, ).…”
Section: Instrumentation Data and Methodsmentioning
confidence: 99%
“…A detailed description of the complex propagation parameter and the complex altitudes can be found in Kulak et al . [].…”
Section: The Methods For Reconstructing the Current Moment Waveformmentioning
confidence: 99%
“…Typical values of h e and h m at 8 Hz for the daytime ionosphere are h e ≈53 km and h m ≈101 km [ Kulak et al , ] and for the nighttime ionosphere h e ≈63 km and h m ≈114 km [ Kułak and Młynarczyk , ]. More information about the characteristic altitudes of the Earth‐ionosphere waveguide, their relationship with the transmission line parameters of the TDTE model and their calculation from the electric and magnetic field components of the radio wave can be found in Kulak et al []. Since the altitudes of the Earth‐ionosphere waveguide depend on frequency, we can expect different behavior of each SR mode during the SID, depending on the ionizing fluxes reaching different regions of the lower ionospheric layers and the local recombination timescales in these layers.…”
Section: Discussionmentioning
confidence: 99%